ArticleScience advances2025
A two-stage mantle plume-sagduction origin of Archean continental crust revealed by water and oxygen isotopes of TTGs.
Article in Science advances, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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Who cites it
6 citing papers in PubMed.
- Ancient plume-reinforced lithosphere modulates present-day crustal fluid migration and deformation.Nature communications · 2026Article
- Coupled sulfur-silicon isotopes reveal supracrustal origin of Archean continents.Nature communications · 2026Article
- Paleoarchean deep crustal hydration and oxidation induced by subduction-driven water recycling.Science advances · 2026Article
- Redox chemistry of early Earth and the origin of life.Communications chemistry · 2026Review
- Dissecting the puzzle of tectonic lid regimes in terrestrial planets.Nature communications · 2025Article
- Origin of continental crust on early Earth.National science review · 2025Article
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Authors and funding
7 authors.
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Abstract
Evolution of Archean continental crust involved partial melting of mafic crust to form the tonalite-trondhjemite-granodiorite (TTG) series. However, crustal generation remains enigmatic with both plate tectonic and non-plate tectonic modes proposed. In this study, we show that zircons from the ~2.5-billion years ago TTGs in the Eastern Block (EB) of the North China Craton have low water contents (median of 263 parts per million) and high δ
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